Number of the records: 1  

Characterization of expandable clay minerals in Lake Baikal sediments by thermal dehydration and cation exchange

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    SYSNO ASEP0021341
    Document TypeJ - Journal Article
    R&D Document TypeJournal Article
    Subsidiary JOstatní články
    TitleCharacterization of expandable clay minerals in Lake Baikal sediments by thermal dehydration and cation exchange
    TitleCharakterizace rozšířených jílových minerálů v usazeninách jezera Bajkal - termální dehydratací a iontovou výměnou
    Author(s) Grygar, Tomáš (UACH-T)
    Bezdička, Petr (UACH-T) SAI, RID, ORCID
    Hradil, David (UACH-T) RID, SAI
    Hrušková, Michaela (UACH-T)
    Novotná, Kateřina (UACH-T)
    Kadlec, Jaroslav (GLU-S) RID, SAI, ORCID
    Pruner, Petr (GLU-S) RID, SAI, ORCID
    Oberhansli, H. (DE)
    Source TitleClays and Clay Minerals. - : Springer - ISSN 0009-8604
    Roč. 53, č. 4 (2005), s. 389-400
    Number of pages12 s.
    Languageeng - English
    CountryUS - United States
    Keywordscation exchange capacity ; Lake Baikal ; Lake Sediments
    Subject RIVCA - Inorganic Chemistry
    R&D ProjectsIAA3032401 GA AV ČR - Academy of Sciences of the Czech Republic (AV ČR)
    CEZAV0Z40320502 - UACH-T (2005-2011)
    AnnotationThe sedimentary series from Academician Ridge, Lake Baikal, eastern Siberia, was examined using cation exchange capacity (CEC) to estimate the amount of expandable clay minerals (ECM) and high-temperature X-ray diffraction (HT-XRD) to determine their basic classification. The comparison of the magnetic susceptibility (MS) at sub-millennial resolution and the delta(18)O record of a reference Atlantic core (ODP 980) was used to create an age model. The most closely studied part of the series covered the major part of the last glacial cycle (120-20 ky BP). The HT-XRD analysis is based on monitoring the course of ECM dehydration with 5 degrees C steps between 25 and 250 degrees C and enabled us to improve the discrimination between ECM, chlorite and micas. The CEC obtained at millennial resolution showed that the neoformation of ECM in warmer periods of the last interglacial was either insignificant or fully compensated by their dissolution or dilution.
    WorkplaceInstitute of Inorganic Chemistry
    ContactJana Kroneislová, krone@iic.cas.cz, Tel.: 311 236 931
    Year of Publishing2006
Number of the records: 1  

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